
Ibrahim M. Yousif- M.Sc. Geology
- Lecturer, Researcher & Education Advisor at University of Bahri
Ibrahim M. Yousif
- M.Sc. Geology
- Lecturer, Researcher & Education Advisor at University of Bahri
Sedimentology & stratigraphic studies. Depositional processes. Reservoir characterization, quality, and models.
About
14
Publications
6,899
Reads
How we measure 'reads'
A 'read' is counted each time someone views a publication summary (such as the title, abstract, and list of authors), clicks on a figure, or views or downloads the full-text. Learn more
40
Citations
Introduction
Ibrahim Yousif works as a university lecturer of petroleum geology and sedimentology at the University of Bahri, Sudan. Experience in outcrop analogue studies, core analysis, petrography, petrology, and reservoir geology in Saudi Arabia and Sudan. Ibrahim is familiar with analyzing siliciclastic and carbonate facies, stratigraphy, reservoir characteristics, quality, and depositional models. The scope of his research is to investigate the characteristics and quality of formations and reservoirs.
Current institution
Additional affiliations
January 2018 - present
University of Bahri (Former Juba University)
Position
- Lecturer
Description
- Instructor of many courses such as straigraphy, sedimentology, Paleontology, Carbonate Geology, Marine Geology, Well Logging, Formation evaluation and Petroleum Geology. Supervision of undergraduate projects. Department Coordinator. Examination Officer.
August 2014 - August 2017
Education
August 2014 - December 2017
September 2006 - August 2011
Publications
Publications (14)
The Aradeiba Formation plays a dual role as both a secondary reservoir and an effective seal in the Muglad Rift Basin, deposited in fluvio-deltaic and lacustrine environments. This study focuses on the Aradeiba D-Sand within the Simbir West oilfield, exploring its sedimentology, heterogeneity, and reservoir quality through a multi-scale approach. B...
The Muglad rift basin is a prolific hydrocarbon sedimentary basin. Determining the relations between petrophysical and sedimentological heterogeneity is critical in reservoir studies. This study aims to integrate analyses of petrophysics and rock physics from the Upper Cretaceous Aradeiba, Zarqa, and Ghazal Formations in Muglad basin to evaluate re...
Traditional approaches to fluvial sedimentary analysis often face challenges in deciphering complex, multivariate data-sets. This study combines compositional data analysis (CoDA) with principal component analysis (PCA) to enhance the characterization of depositional processes and sub-environments within the Shendi Formation. The PCA applied to cen...
The Upper Cretaceous Aradeiba and Bentiu Formations are the two main hydrocarbon reservoirs in the Muglad Basin of Sudan. The basin has NW-SE trend and straddles Sudan and South Sudan republics. Following the cessation of South Sudan from the northern part, the Northern Sudan Republic has lost huge oil reserves. However, some northern Sudanese oil...
4D reservoir monitoring has recently become a major tool used to manage the hydrocarbon production of reservoirs. When combined to production well data, high quality 4D seismic is very useful to address production changes in a reservoir over time. This becomes very challenging though, for most of the clastic reservoirs from the J-Area field, in Cen...
Paleozoic, Mesozoic and Cenozoic carbonate ramp successions are excellently exposed in outcrops in central and eastern regions of Saudi Arabia. These carbonate formations are economically important as hydrocarbon reservoir targets in Saudi Arabia and the Arabian Plate in general. During the Phanerozoic time, the Arabian plate passed through various...
Well exposed Jurassic outcrops belt in central Saudi Arabia provides good outcrop analogs which can be utilized to capture the high resolution facies types and architecture that might help to fill the inter-wells gap in the subsurface. This study is focused on the characterization and modeling the facies types, body geometries deposited in geomorph...
The study aims to identify lithofacies, diagenetic properties, porosity and permeability, compressional and shear wave velocity, rock strength and dynamic elastic moduli of carbonate rocks. All these aspects are used together to delineate the major factors that influences acoustic and geomechanical properties of carbonate rocks of Jurassic Dhruma F...
The well-exposed Jurassic carbonate outcrops in central Saudi Arabia provide an excellent opportunity to characterize the detailed microfacies heterogeneity and stratigraphic architecture within the real inter-well spacing. The current study integrates microfacies and stratigraphic analysis of the D5 and D6 Members in outcrops to define lithofacies...
The well-exposed Jurassic carbonate outcrops in central Saudi Arabia provide an excellent opportunity to characterize the detailed microfacies heterogeneity and stratigraphic architecture within the real inter-well spacing. The current study integrates microfacies and stratigraphic analysis of the D5 and D6 Members in outcrops to define lithofacies...
This study characterizes the lithofacies, paleoenvironment and stratigraphic architecture of the D5 and
D6 members of carbonates Dhruma Formation outcrops in central Saudi Arabia. The study integrates
detailed lithofacies analysis based on vertical and lateral profiles, in addition to thin-sections petrography
to reveal the high-resolution architec...
The study aims to characterize the lithofacies, paleoenvironment, high-resolution
stratigraphic architecture and reservoir characteristics of Dhruma Formation in outcrops in
central Saudi Arabia.
This study investigates the microfacies and sequence stratigraphic frame work of the Middle Jurassic Dhruma Formation in outcrops in central Saudi Arabia. The study contributes to the efforts to understand and enhance local and regional stratigraphic relationship and correlation of the Jurassic carbonate sequences and their significance to reservoi...
Questions
Questions (2)
I have elemental composition from XRF results. I need to know what minerals I have?
How seismic stratigraphy supercided biostratigrahy as subsurface correlative tool? Is that means biostratigrahy no longer more effective tool for subsurface correlation between different wells?